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臭氧-曝气生物滤池深度处理垃圾焚烧渗滤液可行性研究 总被引:6,自引:0,他引:6
研究了臭氧-曝气生物滤池(BAF)代替纳滤和反渗透深度处理垃圾焚烧渗滤液达标排放的技术可行性.半间歇臭氧氧化试验表明,实验用水的可生化性随着氧化时间的增加而增加,色度及UV254, 15min内去除率分别达91%和64%;氧化时间为45min时COD去除率59%, 45min后COD去除较慢, 120min时去除率77%.确定臭氧氧化时间为1h,在同样臭氧浓度与流量下进行了臭氧-BAF处理垃圾焚烧渗滤液的连续实验.结果发现,此工艺对COD、色度和UV254的去除率分别可达75%,95%和90%,其中2/3运行时间里COD低于排放标准100 mg/L.其中出水色度可稳定保持在40度以下达标排放.经过进一步优化,臭氧-BAF有望用于垃圾焚烧渗滤液的达标处理.GC-MS检测表明烷烃,芳香族化合物及含氮杂环化合物是试验用水的主要污染物,臭氧-BAF能够有效去除后两类化合物,但难以去除烷烃. 相似文献
75.
电子废弃物的资源化既能实现资源的二次利用,又能防止环境污染,具有重要的理论意义和应用价值.运用灰色理论对离心复合力场回收废弃电路板金属过程中反冲水、转速和浓度等操作参数对分选效果(精矿品位和精矿的回收率)的影响进行了研究,建立了基于GM(0,N)灰色模型的离心复合力场回收废弃电路板分选模型.经验证模型精度较高. 相似文献
76.
使用单级和两级串联臭氧-生物活性炭(O3-BAC)处理垃圾焚烧渗滤液的二级生物处理尾水,比较研究了污染物去除效果.结果表明,臭氧投加量为200 mg·L-1时,两级串联O3-BAC对COD、UV254和色度的去除率分别为75.9%±2.1%、78.8%±2.9%和96.8%±0.9%,处理出水COD基本保持在100 mg·L-1以下,色度低于40倍,满足GB 16889-2008排放要求;而单级O3-BAC对COD、UV254和色度的去除率分别为68.2%±1.3%、69.7%±0.5%和92.5%±1.1%,处理出水COD和色度分别为150 mg·L-1和60倍,不能达到排放要求.单级O3-BAC在290 mg·L-1臭氧投加量下,才能达到两级串联O3-BAC在200mg·L-1臭氧投加量下的污染物去除效果.此外,两级串联O3-BAC在臭氧投加量200 mg·L-1时的总磷去除率为63.5%±4.4%,出水总磷浓度稳定在1 mg·L-1以下,直接满足GB 16889-2008排放要求. 相似文献
77.
不同基质浓度下SBR进水方式对厌氧氨氧化的影响 总被引:5,自引:0,他引:5
采用厌氧SBR反应器,分别以配水培养和以实际晚期垃圾渗滤液培养的厌氧氨氧化菌为研究对象,考察了不同基质浓度下,SBR改进式连续进水方式与一次性进水方式对厌氧氨氧化工艺运行性能的影响.结果表明,当处理人工配水时,在中低进水浓度下(NO2--N£400mg/L),与改进式连续进水方式相比,宜采用一次性进水方式运行;在高进水浓度下(NO2--N3400mg/L)改进式连续进水方式比一次性进水方式优势明显,特别是在5h改进式连续进水方式下,平均比污泥脱氮速率增加至39.11mgN/(gVSS·h),相比一次进水方式效率提高40%.当处理进水NO2--N浓度为(300±20)mg/L的实际晚期垃圾渗滤液时, 5h改进式连续进水的SBR比污泥脱氮速率最高.由于晚期渗滤液较配水成分复杂,使得厌氧氨氧化菌面临有机物和有害物质的影响,其厌氧氨氧化的反应速率低于同等基质浓度配水条件下的厌氧氨氧化反应速率. 相似文献
78.
采用蒸发-固化工艺处理垃圾渗滤液反渗透浓缩液。蒸发工艺可将反渗透浓缩液减量化,固化工艺可将蒸发残留液中的污染物稳定化。研究表明,蒸发残留液宜采用水泥和石灰混合料进行固化,混合料最佳水泥与石灰质量比约为1︰2,每100 mL蒸发残留液(质量约为120 g)最佳投加量为50 g。固化体含水率低于40%,抗压强度高于1.0 MPa,适合填埋处置,其浸出液污染物含量较低。采用硅酸钠和硫酸钙作为添加剂可加快固化速度,提高固化体的抗压强度。利用蒸发-固化工艺处理反渗透浓缩液可取得良好的经济和社会效益。 相似文献
79.
Michelle M. Lorah Isabelle M. Cozzarelli J.K. Bhlke 《Journal of contaminant hydrology》2009,105(3-4):99-117
The biogeochemistry at the interface between sediments in a seasonally ponded wetland (slough) and an alluvial aquifer contaminated with landfill leachate was investigated to evaluate factors that can effect natural attenuation of landfill leachate contaminants in areas of groundwater/surface-water interaction. The biogeochemistry at the wetland-alluvial aquifer interface differed greatly between dry and wet conditions. During dry conditions (low water table), vertically upward discharge was focused at the center of the slough from the fringe of a landfill-derived ammonium plume in the underlying aquifer, resulting in transport of relatively low concentrations of ammonium to the slough sediments with dilution and dispersion as the primary attenuation mechanism. In contrast, during wet conditions (high water table), leachate-contaminated groundwater discharged upward near the upgradient slough bank, where ammonium concentrations in the aquifer where high. Relatively high concentrations of ammonium and other leachate constituents also were transported laterally through the slough porewater to the downgradient bank in wet conditions. Concentrations of the leachate-associated constituents chloride, ammonium, non-volatile dissolved organic carbon, alkalinity, and ferrous iron more than doubled in the slough porewater on the upgradient bank during wet conditions. Chloride, non-volatile dissolved organic carbon (DOC), and bicarbonate acted conservatively during lateral transport in the aquifer and slough porewater, whereas ammonium and potassium were strongly attenuated. Nitrogen isotope variations in ammonium and the distribution of ammonium compared to other cations indicated that sorption was the primary attenuation mechanism for ammonium during lateral transport in the aquifer and the slough porewater. Ammonium attenuation was less efficient, however, in the slough porewater than in the aquifer and possibly occurred by a different sorption mechanism. A stoichiometrically balanced increase in magnesium concentration with decreasing ammonium and potassium concentrations indicated that cation exchange was the sorption mechanism in the slough porewater. Only a partial mass balance could be determined for cations exchanged for ammonium and potassium in the aquifer, indicating that some irreversible sorption may be occurring.Although wetlands commonly are expected to decrease fluxes of contaminants in riparian environments, enhanced attenuation of the leachate contaminants in the slough sediment porewater compared to the aquifer was not observed in this study. The lack of enhanced attenuation can be attributed to the fact that the anoxic plume, comprised largely of recalcitrant DOC and reduced inorganic constituents, interacted with anoxic slough sediments and porewaters, rather than encountering a change in redox conditions that could cause transformation reactions. Nevertheless, the attenuation processes in the narrow zone of groundwater/surface-water interaction were effective in reducing ammonium concentrations by a factor of about 3 during lateral transport across the slough and by a factor of 2 to 10 before release to the surface water. Slough porewater geochemistry also indicated that the slough could be a source of sulfate in dry conditions, potentially providing a terminal electron acceptor for natural attenuation of organic compounds in the leachate plume. 相似文献
80.
太阳光Fenton法处理垃圾渗滤液中有机污染物 总被引:6,自引:1,他引:6
研究利用太阳光Fenton法处理垃圾渗滤液。根据太阳光辐射强度随时间的变化规律,选择重庆7、8月份的晴天,在中午12:00到下午14:00时进行试验,研究太阳光辐射时间、pH值、Fenton试剂用量对垃圾渗滤液COD去除率的影响。研究结果表明:太阳光Fenton法对垃圾渗滤液的COD有较好的去除效果,COD去除率达86.2%。太阳光Fenton法处理垃圾渗滤液的优化条件是:日光辐射时间为120 min,pH值为2.5,Fe2+浓度为5 mmol/L,H2O2浓度为570 mmol/L。同时,论文还对太阳光Fenton法处理垃圾渗滤液的动力学进行分析。研究结果显示:太阳光Fenton法处理垃圾渗滤液,其表观动力学方程为-dC/dt=2.6×10-8×P1.92×F1.79×E1.67。 相似文献